Sibert, Elizabeth C; Hull, Pincelli M; Norris, Richard D (2014): Ichthyolith counts and MAR at Gubbio outcrop [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.834230, In supplement to: Sibert, EC et al. (2014): Resilience of Pacific pelagic fish across the Cretaceous/Palaeogene mass extinction. Nature Geoscience, 7(9), 667-670, https://doi.org/10.1038/ngeo2227
Always quote citation above when using data! You can download the citation in several formats below.
Further details:
Lowrie, William; Alvarez, Walter (1977): Upper Cretaceous–Paleocene magnetic stratigraphy at Gubbio, Italy III. Upper Cretaceous magnetic stratigraphy. Geological Society of America Bulletin, 88(3), 374-377, https://doi.org/10.1130/0016-7606(1977)88%3C374:UCMSAG%3E2.0.CO;2
Monechi, Simonetta; Thierstein, Hans R (1985): Late Cretaceous-Eocene nannofossil and magnetostratigraphic correlations near Gubbio, Italy. Marine Micropaleontology, 9(5), 419-440, https://doi.org/10.1016/0377-8398(85)90009-X
Mukhopadhyay, Sujoy; Montanari, Alessandro; Farley, Kenneth A (2001): A Short Duration of the Cretaceous-Tertiary Boundary Event: Evidence from Extraterrestrial Helium-3. Science, 291(5510), 1952-1955, https://doi.org/10.1126/science.291.5510.1952
Premoli Silva, Isabella (1977): Upper Cretaceous–Paleocene magnetic stratigraphy at Gubbio, Italy II. Biostratigraphy. Geological Society of America Bulletin, 88(3), 371-374, https://doi.org/10.1130/0016-7606(1977)88%3C371:UCMSAG%3E2.0.CO;2
Sibert, Elizabeth C; Hull, Pincelli M; Norris, Richard D (2014): Age model of Gubbio outcrop [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.834214
Coverage:
Latitude: 43.360000 * Longitude: 12.580000
Minimum SECTION, height: 343.83 m * Maximum SECTION, height: 355.43 m
Comment:
DEPTH, sediment/rock [m] is given in mbsf. All Ichthyolith counts were collected as part of this study. The primary age model was developed using biostratigraphic and magnetostratigraphic markers (see Gubbio Age model for details) and age datums from GTS 2012. A second age model (a helium age model) was used to test the sensitivity of our conclusions to age models affects. Helium sedimentation rates were directly taken from Figure 2 of Mukhopadhyay et al. (2001). The Gubbio K/Pg boundary is at 347.63 m (GTS 2012 boundary age = 66.04 Ma). MAR were calculated using a constant dry bulk density of 2.7g/cm^3 in both cases.
Parameter(s):
| # | Name | Short Name | Unit | Principal Investigator | Method/Device | Comment |
|---|---|---|---|---|---|---|
| 1 | Sample code/label | Sample label | Sibert, Elizabeth C | |||
| 2 | Depth, relative | Depth rel | m | Sibert, Elizabeth C | relative to K/Pg (m) | |
| 3 | SECTION, height | Section | m | Geocode | ||
| 4 | AGE | Age | ka BP | Geocode | ||
| 5 | Ichthyoliths | Ichthyol | # | Sibert, Elizabeth C | Counting >38 µm fraction | |
| 6 | Dry mass | Dry m | g | Sibert, Elizabeth C | ||
| 7 | Ichthyoliths | Ichthyol | #/g | Sibert, Elizabeth C | Counting >38 µm fraction | |
| 8 | Accumulation rate, mass | MAR | g/cm2/ka | Sibert, Elizabeth C | ||
| 9 | Accumulation rate, ichthyoliths | Acc rate ichthyol | #/cm2/ka | Sibert, Elizabeth C | Counting >38 µm fraction | |
| 10 | Age model, optional | Age model opt | ka | Sibert, Elizabeth C | rough est. He MARs | |
| 11 | Accumulation rate, mass | MAR | g/cm2/ka | Sibert, Elizabeth C | rough est. He MARs | |
| 12 | Accumulation rate, ichthyoliths | Acc rate ichthyol | #/cm2/ka | Sibert, Elizabeth C | Counting >38 µm fraction | rough est. He MARs |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
341 data points